Secondary organic aerosol formation from nitrate radical oxidation of styrene: aerosol yields, chemical composition, and hydrolysis of organic nitrates
<p>Styrene is emitted by anthropogenic sources and biomass burning and is highly reactive towards atmospheric oxidants. While it has the highest nitrate radical (NO<span class="inline-formula"><sub>3</sub></span>) reactivity among aromatic hydrocarbons, the NO...
| Published in: | Atmospheric Chemistry and Physics |
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| Main Authors: | , , , , |
| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2025-05-01
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| Online Access: | https://acp.copernicus.org/articles/25/5215/2025/acp-25-5215-2025.pdf |
| Summary: | <p>Styrene is emitted by anthropogenic sources and biomass burning and is highly reactive towards atmospheric oxidants. While it has the highest nitrate radical (NO<span class="inline-formula"><sub>3</sub></span>) reactivity among aromatic hydrocarbons, the NO<span class="inline-formula"><sub>3</sub></span> oxidation of styrene and formation mechanisms of secondary organic aerosols (SOA) have not been investigated. In this study, we conduct chamber experiments with styrene concentrations ranging from 9.5 to 155.2 ppb. The resulting SOA yields range from 14.0 % to 22.1 % with aerosol mass loadings of 5.9–147.6 <span class="inline-formula">µ</span>g m<span class="inline-formula"><sup>−3</sup></span> after wall loss corrections. The chemical composition of SOA is characterized by online measurements, revealing that dimeric organic nitrates (ONs) constitute 90.9 % of the total signal of particle-phase products. C<span class="inline-formula"><sub>16</sub></span>H<span class="inline-formula"><sub>16</sub></span>N<span class="inline-formula"><sub>2</sub></span>O<span class="inline-formula"><sub>8</sub></span> and C<span class="inline-formula"><sub>8</sub></span>H<span class="inline-formula"><sub>9</sub></span>NO<span class="inline-formula"><sub>4</sub></span> are identified as the major particle-phase products, which constitute 88.3 % and 4.1 %, respectively, of the measured signal. We propose formation mechanisms for the ON products, including the common RO<span class="inline-formula"><sub>2</sub>+</span> RO<span class="inline-formula"><sub>2</sub></span> <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M14" display="inline" overflow="scroll" dspmath="mathml"><mo>/</mo></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="8pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="539a58614ea8688159b8effbc6d3da8d"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="acp-25-5215-2025-ie00001.svg" width="8pt" height="14pt" src="acp-25-5215-2025-ie00001.png"/></svg:svg></span></span> HO<span class="inline-formula"><sub>2</sub></span> pathway and other radical chain termination reactions such as RO <span class="inline-formula">+</span> R and R <span class="inline-formula">+</span> R. We also investigate the hydrolysis of particulate ONs. The hydrolysis lifetime for ONs is determined to be less than 30 min. This short hydrolysis lifetime can be attributed to the stabilization of the carbocation by delocalized <span class="inline-formula"><i>π</i></span> orbitals of the benzene-related skeleton of aromatic ONs. This work provides the first fundamental laboratory data to evaluate SOA production from styrene <span class="inline-formula">+</span> NO<span class="inline-formula"><sub>3</sub></span> chemistry. Additionally, the formation mechanisms of aromatic ONs are reported for the first time, highlighting that compounds previously identified as nitroaromatics in ambient field campaigns could also be attributed to aromatic ONs.</p> |
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| ISSN: | 1680-7316 1680-7324 |